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Diamond Head

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Journal Article
Published: 01 December 1937
Journal of Sedimentary Research (1937) 7 (3): 91–103.
...Chester Keeler Wentworth Abstract Black ash or cinders from explosive volcanic eruptions form conspicuous surficial deposits in the Tantalus, Makiki, and other parts of Honolulu. The fine-grained black sand deposits southeast of Diamond Head and along the Black Point coast have long been considered...
Journal Article
Journal: GSA Bulletin
Published: 01 January 1906
GSA Bulletin (1906) 17 (1): 469–484.
...C. H. HITCHCOCK Abstract Introduction The title of the paper presented at Ottawa is “Hawaiian Notes.” These naturally grouped themselves into three parts: First, the facts observed in Oahu, particularly about Diamond head; second, the further study of the supposed caldera at Mokohea; and, third...
Image
(A)  The <span class="search-highlight">Diamond</span> <span class="search-highlight">Head</span> and Waikiki coast on the southern shore of Oahu is an...
Published: 01 March 2001
FIGURE 2 (A) The Diamond Head and Waikiki coast on the southern shore of Oahu is an example of a developed coastal plain beach with a broad fringing reef tract (D/Bbrfr). (B) Along the northeastern coast of Molokai, embayments comprised of a stream mouth and beach (S/B) are often interspersed
Journal Article
Published: 01 August 2011
Bulletin of the Seismological Society of America (2011) 101 (4): 1742–1758.
... of microearthquakes are found to occur near Oahu. There is no evidence from our analyses that the Molokai fracture zone ( MFZ ) is seismically active at this time, and no evidence was found of a previously hypothesized Diamond Head fault ( DHF ) near Oahu. However, on the basis of both the PLUME and HVO locations...
FIGURES | View All (11)
Journal Article
Journal: GSA Bulletin
Published: 01 May 1971
GSA Bulletin (1971) 82 (5): 1399–1404.
... Hawaiian landmarks as Diamond Head and Punchbowl. Ages vary from about 30,000 yrs for the Koko rift zone lavas to about 800,000 yrs for the oldest member measured (Castle flow). HAWAII INSTITUTE.OF GEOPHYSICS CONTRIBUTION No. 383 18 12 1970 Copyright © 1971, The Geological Society...
Image
Location of large ( M ≥6) historical (1823–2005) earthquakes (circles) in t...
Published: 01 August 2011
of Hawaii, shown as relief illuminated from the south, are taken from an updated version of the map of Eakins et al. (2003) . The locations of the Molokai fracture zone ( MFZ ) from Müller et al. (1997) and the hypothesized Diamond Head fault ( DHF ) from Furumoto et al. (1980) are indicated
Journal Article
Published: 01 March 1997
Seismological Research Letters (1997) 68 (2): 277–336.
... Meeting Place Hawaiian Regent Hotel
 2552 Kalakaua Avenue
 Honolulu, Hawaii Oral Sessions—Koa, Kamani, and Kukui Rooms
 Poster Sessions—Diamond Head Ballroom
 Exhibits, Computer Demonstrations, and Refreshments—Diamond Head Ballroom Registration Information Registration information...
Image
Cephalic morphometrics of gynes for relevant fossil  Gesomyrmex  species. (...
Published: 02 February 2023
Fig. 4. Cephalic morphometrics of gynes for relevant fossil Gesomyrmex species. (a) Head length (HL). (b) Normalized head shape (head length/head width, HRN, squares) and normalized relative eye diameter (eye diameter/head length, HERN, diamonds). Abbreviations: flav. , flavescens ; germ
Journal Article
Published: 27 March 2009
Canadian Journal of Earth Sciences (2009) 46 (2): 139–154.
... that the shallow lithospheric mantle may be too oxidized to contain graphite. Other diamond-bearing regions show no upper mantle conductor suggesting that the correlation with diamondiferous kimberlites is not universal. The Buffalo Head Hills in Alberta host diamondiferous kimberlites in a Proterozoic terrane...
FIGURES | View All (4)
Journal Article
Published: 21 June 2008
Canadian Journal of Earth Sciences (2008) 45 (5): 513–529.
... generally occurs in the northwestern part of the field and defines the diamond window for the Buffalo Head Hills kimberlite field. This volcanism is contemporaneous with sedimentary host rock deposition, which has important implications for the size and morphological complexity of the kimberlite bodies...
FIGURES
Journal Article
Journal: Geology
Published: 04 August 2017
Geology (2017) 45 (10): 871–874.
... show evidence of fluid exsolution only in CK-A and MVK lithologies, but no fluid presence in CK-B. The observed diamond resorption features may be controlled by (1) a temporary separation of the rising magma column into a bubble-rich head and bubble-poor volatile-depleted tail and (2) fluid exsolution...
FIGURES
Journal Article
Journal: Economic Geology
Published: 01 August 1999
Economic Geology (1999) 94 (5): 749–758.
... sizes of 1.1 to 1.3 ct/stn) and bar heads (0.7 to 1.5 cpht and average stone sizes of 1 to 1.3 ct/stn) while bar tails are practically barren. Although the vertical decline in diamond concentration may be attributed to a decrease in diamond supply during the aggradation of the Proto-Orange gravels...
Series: Geological Society, London, Special Publications
Published: 15 March 2021
DOI: 10.1144/SP506-2020-11
EISBN: 9781786209931
... and Natalia Sarsadskhih. Natalia was the head of the mineralogical laboratory who implemented a new methodology to search for mineral indicators of primary diamond deposits. Larisa was a young geologist who joined Natalia's team in 1953. The work of these women led to the discovery, in 1954, of the first...
FIGURES | View All (8)
Image
Details of the sample, <span class="search-highlight">diamond</span> anvils, heaters, and electric circuits for h...
Published: 01 September 2003
Fig. 1. Details of the sample, diamond anvils, heaters, and electric circuits for heating, controlling, and measuring the temperature of the sample in the hydrothermal diamond anvil cell (HDAC). Fig. 2. The hydrothermal diamond anvil cell (HDAC). The three guide posts and three driver screws
Image
Details of the sample, <span class="search-highlight">diamond</span> anvils, heaters, and electric circuits for h...
Published: 01 September 2003
Fig. 1. Details of the sample, diamond anvils, heaters, and electric circuits for heating, controlling, and measuring the temperature of the sample in the hydrothermal diamond anvil cell (HDAC). Fig. 2. The hydrothermal diamond anvil cell (HDAC). The three guide posts and three driver screws
Image
Plan view of the receiver array at the Barnett Shale reservoir; red and blu...
Published: 01 December 2012
Figure 1. Plan view of the receiver array at the Barnett Shale reservoir; red and blue denote the central and outer part of the array, respectively. The two black lines denote the horizontal wells. The filled black diamond represents the well head and the empty black diamonds represent the well
Image
Backscattered electron images of cosmic spherules (CS), with equal area ste...
Published: 01 February 2011
Figure 2. Backscattered electron images of cosmic spherules (CS), with equal area stereograms of magnetization (black diamond—lower hemisphere; white diamond—upper hemisphere; small circle—95% confidence angle), and fall vector (black-headed arrow—lower hemisphere; white-headed arrow—upper
Journal Article
Published: 01 June 2016
Russ. Geol. Geophys. (2016) 57 (6): 858–867.
... that fail to reach the surface; intermediate, Ka from 1.15 to 1.9, plumes that erupt on the surface; high, Ka from 1.9 to 10, plumes with mushroom–shaped heads. While on the subject of diamondiferous plumes, we assume the possibility of diamond crystals existing in the magmatic melt in the plume...
FIGURES | View All (10)
Image
Same as Figure  11 , but the <span class="search-highlight">diamonds</span> mark the critical angle estimated fro...
Published: 16 March 2007
Figure 12. Same as Figure 11 , but the diamonds mark the critical angle estimated from the horizontal velocity of the head wave.
Image
Sketch of the ablation <span class="search-highlight">head</span>. The spatial filter (SF) consists of a 50 μm di...
Published: 01 November 2000
Fig. 1. Sketch of the ablation head. The spatial filter (SF) consists of a 50 μm diameter hole in diamond onto which the laser beam is focused with lens L 1 .